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Suðurnes
Southern Peninsula (, ) is an administrative unit and part of Reykjanesskagi (pronounced ), or Reykjanes Peninsula, a region in southwest Iceland. It was named after Reykjanes, the southwestern tip of Reykjanesskagi. The region has a population of 30,933 (2024) and is one of the more densely populated parts of the island. The administrative centre is Keflavík, which had 7,000 residents when it merged with the nearby town of Njarðvík and Hafnir in 1995 to create Reykjanesbær, which is the largest settlement outside the Greater Reykjavík area; in 2018, the region had a population of 17,805. The region is the location of Keflavík International Airport, the major point of entry for Iceland. Some fishing towns, such as Grindavík, Njarðvík and Sandgerði, are situated on the peninsula. The peninsula is marked by active volcanism under its surface and large lava fields, allowing little vegetation. There are numerous hot springs in the southern half of the peninsula, around t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reykjanesbær
Reykjanesbær () is a municipality on the Southern Peninsula (''Suðurnes'') in Iceland, though the name is also used by locals to refer to the suburban region of Keflavík and Njarðvík which have grown together over the years. The municipality is made up of the towns of Keflavík and Njarðvík and the village of Hafnir. The municipality was created in 1994 when the inhabitants of the three settlements voted to merge them into one. Reykjanesbær is the fourth largest municipality in Iceland, with 21.957 citizens (2024). Overview Of the three towns which make up the municipality, Keflavík is the largest, while Hafnir is the smallest and some 10 kilometers distant. Keflavík and Njarðvík were originally distinct towns but gradually grew together over the course of the latter half of the 20th century, until the only thing separating them was a single street. The northern side of the street belonged to Keflavík and the southern side to Njarðvík. Since May 2009 the township ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandgerði
Sandgerði (), also known as Sandgerðisbær (, ), is a town in southwestern Iceland on the Southern Peninsula Southern Peninsula (, ) is an administrative unit and part of Reykjanesskagi (pronounced ), or Reykjanes Peninsula, a region in southwest Iceland. It was named after Reykjanes, the southwestern tip of Reykjanesskagi. The region has a populati .... It is part of the municipality of Suðurnesjabær, formed in 2018 when it merged with Garður. Sandgerði began to develop as a fishing village in the second half of the nineteenth century as motorboats replaced row boats in the industry. Knattspyrnudeild Reynis, Reynir football club play in Iceland's third tier and their basketball team by the same name competes in the 3rd tier of basketball in Iceland as well. Suðurnes Science and Learning Center is a museum and research center dedicated to natural science and related subjects. References External links Official site More information and photos about Sandgerði o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Regions Of Iceland
The regions of Iceland are eight areas of Iceland that roughly follow the arrangement of parliamentary constituencies as they were between 1959 and 2003. These regions are not incorporated polities but rather recognized groupings of municipalities. Iceland only has two levels of administration, the national government and 62 municipalities. The municipalities have organized themselves into eight regional associations and those boundaries are also recognized by Statistics Iceland to report statistics. Since 2014, police and commissioner ('' sýslumaður'') districts have followed the eight region model with the exception that Vestmannaeyjar forms a special district and not part of the Southern Region. The divisions of Iceland for the purposes of health care and district courts diverge more from the commonly used eight region model. The postal code system also roughly corresponds with the regions with the first digit of the three digit codes usually being the same as on the map b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reykjanes
Reykjanes () is a small headland on the south-western end of the Reykjanes Peninsula in Iceland, giving the main peninsula its name. Volcanic action is responsible for forming the entire peninsula. The nearest town is Keflavik. The name, , translates to "smoking point,” , and . It is named this due to the continuing volcanic activity of the Reykjanes volcanic belt; there are also many other uses of this name in Iceland, e.g. the Reykjanes Peninsula or Reykjanes in Ísafjarðardjúp. Geography The region is about to the south of Keflavík International Airport, Iceland's international airport. It is about and includes the Reykjanes volcanic system that extends in a linear fashion up its centre continuing to the north-east as the hill of Sýrfell at high. Other volcanic systems of the Reykjanes volcanic belt could affect the Reykjanes region and have erupted as recently as April 2025. Other hills associated with the system are Skálafell (Grindavíkurbær) with a height of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Keflavík International Airport
Keflavík Airport ( ) , also known as Reykjavík–Keflavík Airport, is the largest airport in Iceland and the country's main airline hub, hub for international transportation. The airport is located approximately west of the town of Keflavík, Reykjanesbær and southwest of the capital Reykjavík. The airport has two runways, each measuring approx. . Most international journeys to or from Iceland pass through this airport. Keflavík is a Airline hub, hub for Icelandair and the airline Play (airline), Play. The airport is only used for international flights; all domestic flights use the smaller Reykjavík Airport, which lies from Reykjavík's city centre. Keflavík Airport is operated by Isavia, a government enterprise. History Early years Originally, the airport was built by the United States military during the Allied occupation of Iceland, military allied occupation of Iceland in World War II, as a replacement for a small British landing strip at Garður to the nort ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blue Lagoon (geothermal Spa)
The Blue Lagoon ( ) is a geothermal spa in southwestern Iceland. The spa is located in a lava field from Grindavík and in front of Mount Þorbjörn on the Reykjanes Peninsula, in a location favourable for geothermal power, and is supplied by water used in the nearby Svartsengi geothermal power station. The Blue Lagoon is approximately from Keflavík International Airport, and is one of the most visited tourist attractions in Iceland. Description The water's milky blue hue is due to its high silica content. The silica forms soft white mud on the bottom of the lake which bathers rub on themselves. The water is also rich in salts and algae. The water temperature in the bathing and swimming area of the lagoon averages . Guests are required to shower in the nude prior to using the geothermal spa. The communal showers are split up by gender. Children aged eight and under are only allowed entry with the use of arm floaters, provided free of charge. The lagoon is not suitable ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rift Valley
A rift valley is a linear shaped lowland between several highlands or mountain ranges produced by the action of a geologic rift. Rifts are formed as a result of the pulling apart of the lithosphere due to extensional tectonics. The linear depression may subsequently be further deepened by the forces of erosion. More generally the valley is likely to be filled with sedimentary deposits derived from the rift flanks and the surrounding areas. In many cases rift lakes are formed. One of the best known examples of this process is the East African Rift. On Earth, rifts can occur at all elevations, from the sea floor to plateaus and mountain ranges in continental crust or in oceanic crust. They are often associated with a number of adjoining subsidiary or co-extensive valleys, which are typically considered part of the principal rift valley geologically. Earth's rift valleys The most extensive rift valley is located along the crest of the mid-ocean ridge system and is the result ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Leif Erikson
Leif Erikson, also known as Leif the Lucky (), was a Norsemen, Norse explorer who is thought to have been the first European to set foot on continental Americas, America, approximately half a millennium before Christopher Columbus. According to the sagas of Icelanders, he established a Norse colonization of North America, Norse settlement at Vinland, which is usually interpreted as being coastal North America. There is ongoing speculation that the settlement made by Leif and his crew corresponds to the remains of a Norse settlement found in Newfoundland, Canada, called L'Anse aux Meadows, which was occupied approximately 1,000 years ago. Leif's place of birth is unknown, although it is assumed to have been in Iceland.Leif Eriksson – Encyclopædia Britannica, Inc., 2012. Retrieved 11 April 2012. His fat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plate Tectonics
Plate tectonics (, ) is the scientific theory that the Earth's lithosphere comprises a number of large tectonic plates, which have been slowly moving since 3–4 billion years ago. The model builds on the concept of , an idea developed during the first decades of the 20th century. Plate tectonics came to be accepted by Earth science, geoscientists after seafloor spreading was validated in the mid-to-late 1960s. The processes that result in plates and shape Earth's crust are called ''tectonics''. Tectonic plates also occur in other planets and moons. Earth's lithosphere, the rigid outer shell of the planet including the crust (geology), crust and upper mantle, is fractured into seven or eight major plates (depending on how they are defined) and many minor plates or "platelets". Where the plates meet, their relative motion determines the type of plate boundary (or fault (geology), fault): , , or . The relative movement of the plates typically ranges from zero to 10 cm annu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
